Umbrella structure and channel-wall stoping in the Cambrian St. Roch Formation, Quebec Appalachians: significance for particle support mechanisms and turbulence development in hyper-concentrated sediment gravity flows
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
http://link.springer.com/content/pdf/10.1007/s00531-013-0968-3.pdf
Reference40 articles.
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3. Bagnold RA (1956) The flow of cohesionless grains in fluids. Royal Soc Lond Phil Trans Series A249:235–297
4. Breien H, de Blasio FV, Elverhøi A, Nystuen JP, Harbitz CB (2010) Transport mechanisms of sand in deep-marine environments—insights based on laboratory experiments. J Sediment Res 80:975–990
5. Gani MR (2004) From turbid to lucid: a straightforward approach to sediment gravity flows and their deposits. Sediment Record 2:4–8
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1. Characterization of carbonate veins in graywacke layers from the Humber zone (Quebec, Canada) and implications for strength recovery of damaged rocks by mineral precipitation;Tectonophysics;2023-12
2. Quartz arenites of the Cambro–Ordovician Kamouraska Formation, Quebec Appalachians, Canada: II. Eolian sands in deep-sea sedimentary gravity-flow deposits;Canadian Journal of Earth Sciences;2015-04
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